Internal Processes Flashcards

1
Q

Divergent boundary

A

1) Magma rises between two plates –> going away from each other
2) EITHER midocean ridge OR continental rift

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2
Q

Convergent boundary

A

1) plates colliding, destructive boundaries
2) lead to orogenesis (mountain building)
3) 3 types: oceanic-continental, oceanic-oceanic, continental-continental

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3
Q

Oceanic-continental convergence

A

1) Oceanic plate goes into asthenosphere of continental
2) Features: creates oceanic trench + volcanic mountains on continental crust

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4
Q

Oceanic-Oceanic Convergence

A

1) More dense oceanic crust subducts
2) Water involved –> cool magma, produces felsic
3) Key Features = oceanic trench, volcanic arc

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5
Q

Continental Continental Convergence

A

1) No subduction because continental crust too buoyant
2) creates huge mountain ranges like himalayas

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6
Q

Transform boundaries

A

1) plates slide laterally –> no new crust created or old crust destroyed
2) found in midocean ridges + in California

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7
Q

Two additions to plate tectonic theory

A

1) hot spots
2) accreted terranes

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8
Q

Hot Spots

A

1) Explains the formation of volcanic islands and seamount chains away from tectonic plate boundaries.
2) A hotspot is a stationary mantle plume that creates volcanic activity as tectonic plates move over it, creating a chain

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9
Q

Accreted terrane

A

1) Fragment of crustal material added to a tectonic plate, found at convergent plate boundaries.
2) explains why plate can have very different sections w. diff geologic features

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10
Q

Volcanic Distribution

A

1) found in areas of convergence
2) Ring of Fire (andesite line)
3) considered active if erupted once within historical times + likely to erupt again

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11
Q

benefits of volcanoes

A

1) most of water on earth today released as water vapor during volcanic eruptions
2) magma contains phosphorus, K, Ca, Mg

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12
Q

4 types of volcanoes

A

Shield, composite/strato, cinder cone, lava dome

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13
Q

Shield volcanoes

A

1) broad + gently sloping mountain, much broader than tall
2) made of layers of solidified lava flows
3) basaltic magma + fluid lava

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14
Q

Composite volcano

A

1) steep sided symmetrical cone
2) made of layers of lava, pyroclastics (ash/cinder), hardened volcanic mudflow
3) explosive + effusive eruptions
4) more felsic + viscous –> makes explosive

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15
Q

Lava Dome (Plug Dome)

A

1) small, irregular shape
2) made of solidified lava that was thick/viscous when molten
3) magma high in silica, explosive eruptions

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16
Q

Cinder Cone

A

1) small, steep-sided cone
2) loose pyroclastics (ash/cinder)
3) baslatic magma, short life span
4) extremely explosive

17
Q

Caldera

A

immense basin-shaped depression (circular) with diameter much larger than volcano vent forms post eruption
ex: crater lake

18
Q

Volcanic Hazards

A

1) Volcanic gases = sudden release of carbon dioxide + sulfur dioxide dangerous –> lead to acid rain + reduce insolation
2) lava flows –> not that dangerous BUT lava flows from intermediate/high silica magma dangerous because explosive
3) eruption column - large fragments of rock - called volcanic bombs - drop to ground + lots of ash falls
4) pyroclastic flow - high speed avalanche of searing hot gases, ash, rock
5) volcanic mudflows - caused when hot ash mixes with water/melting snow –> produces slurry of mud/boulders

19
Q

Types of folding

A

1) Anticline
2) Syncline

20
Q

Anticline

A

1) symmetrical upfold - creates mountains
2) Sad face parabolas

21
Q

syncline

A

1) symmetrical downfold - creates valleys
2) Happy face parabola

22
Q

Two types of tectonism

A

1) folding = crustal rocks become deformed because of lateral compression
2) faulting = rock structure is broken + one is forcibly displaced by other

23
Q

Types of faults

A

1) Normal faults
2) reverse fault
3) thrust faults
4) strike-slip

24
Q

Earthquake

A

1) vibration in Earth produced by shock waves caused from sudden displacement along fault

25
Q

Earthquake dangers

A

1) Ground shaking –> liquefaction + breaking of buildings
2) landslides
3) tsunami = if underwater earthquake

26
Q

Hanging wall vs footwall

A

1) Hanging wall = plate that is moving (on right)
2) footwall = plate the stays still (on left)

27
Q

Normal Fault

A

1) Normal faults = (GOING APART) tension stresses (pulling apart) –> produces steeply inclined fault zone

28
Q

Reverse Fault

A

1) reverse fault = (COMING TOGETHER) compression stresses (pushing together), one block slides UP incline
2) hanging wall pushed up

29
Q

Thrust Fault (don’t need to know)

A

1) thrust faults = Earth’s crust where one piece of rock is pushed up and over another at shallow angle (less than 30 degrees)

30
Q

Strike Slip Fault

A

1) strike-slip = lateral movement